1. Fig. 1.1. An extra neutron in the 13 C isotope makes the nucleus more massive or “heavier” than the 12 C isotope, but does not affect most chemistry that is related to reactions in the electron shell.

2. Fig. 1.2. An abbreviated periodic table of the elements. Elements have more than one isotope variety that differ in the number of neutrons. Stable isotopes of the circled HCNOS elements (hydrogen, carbon, nitrogen, oxygen and sulfur) are emphasized in this book. Details about isotopes for many of these elements are available at the website http://wwwrcamnl.wr.usgs.gov/isoig/period/. http://wwwrcamnl.wr.usgs.gov/isoig/period/

3. Fig. 1.3. You are what you eat - stable isotopes in a 50 kg human who is composed of mostly of light isotopes with a small amount of heavy isotopes. People are mostly water, so hydrogen and oxygen isotopes dominate at >35kg. Next come C isotopes at >11 kg, then N isotopes. S isotopes are missing – they should be here at about 220g for the light isotope 32S and 10g for the heavy isotope 34S. Have you had your isotopes today? (from Wada and Hattori, 1990; reproduced with permission of CRC Press LLC).

4. Fig. 1.4. This book focuses on the five elements (hydrogen, carbon, nitrogen, oxygen and sulfur) and their 13 stable isotopes.

5. Fig. 1.5. Stable isotopes are especially valuable for studying the origins and cycling of organic matter in the biosphere. Ecologists also use radioisotopes (especially 3 H, 14 C, and 32 P) to study cycling rates and to determine ages. Where possible, stable isotopes that pose no health risk are increasingly substituted for the radioisotopes.

6. Fig. 1.6. The extra neutron does make a very slight difference in some reactions; having an extra neutron usually results in slower reactions. This reaction difference is fractionation.

7. Fig. 1.7. The two main themes of the book are fractionation and mixing. Fractionation splits apart mixtures to form source materials. These sources recombine via mixing. There is a strong general analogy between isotopes and colors, so that isotopes can be thought of as dyes or tracers. In this color example, fractionation separates green into yellow and blue components, with conversely yellow and blue mix to form green.

8. Fig. 1.8. Fractionation and mixing together control isotope cycling and circulation. There are many words to use when thinking about isotope “fractionation” or “mixing”, and as long as you remember that these words do not imply human intervention, control or intent, most of these words can help you understand isotope cycling.

9. Fig. 1.9. Isotopes cycle via fractionation and mixing, with fractionation splitting apart mixtures to form source materials. These sources recombine via mixing to complete the cycle.